I
woke up after 4 am to complete certain documentation before the Icefields
Parkway tour pick up. When I was at it I noticed a few elk feeding on the grass
in the YWCA compound. They seemed voraciously hungry and ready to feed on all
the grass in the area. The elk belongs to the deer family but is bigger than a
stag but smaller than a moose. After breakfast of muesli, milk and oranges I
was ready for the fantasy experience. The pick-up vehicle arrived after 8 am
and it was from Banff Tours. There were four couples besides me in the 24-seater
bus and the driver cum guide, Neil, introduced himself at some length when we
started the trip. He also asked us to briefly mention our names and where we
came from. Two families were from Australia and two other from UK.
Along
the 160 plus km to the Athabasca Glacier Neil kept supplying nuggets of
information about the National Parks and a lot more. I think a brief recap of
them is in order. The Banff National Park is the oldest in Canada, having been
established in 1885 and covering over 6500 square km in the Canadian Rocky
Mountains. The park has numerous river systems, glaciers, coniferous forests
and ice fields. The Icefields Parkway, the tour of which I was doing, stretched
from Lake Louise to Jasper National Park. The setting up of the park was almost
co-terminus with the building of the CP railway system from the West to the
East through the Rockies. Presently the National Park along the highway is
fully fenced to avoid any animals being killed – casualty rate was 200 animals
per annum before the fencing. However, the highway cut the park into two.
Therefore, to provide a seamless ecosystem to the animals 4 over passes and 38
tunnels were set up for the animals to cross from one side to the other without
fear of being hurt or killed. The movement of animals is monitored using sensor
triggered cameras, special sand that capture paw prints and barbed wire that
takes fur samples.
The
TCH is reportedly the longest paved highway in the world and the heavy traffic
on the highway is considered to be the highest through any national park in the
world. All through the drive Neil pointed out various mountains and added
information about it. One such was about the Castle Mountain. Apparently during
the visit of D.Eisenhower, the former President of USA, to Canada the Castle
Mountain was renamed Eisenhower Peak. Soon there was a public outcry against
the renaming as the President had spent his time playing golf than even caring
to visit the peak. Castle Mountain soon got back its original name.
The
Columbia Icefields is a large expanse of 325 square km having depths ranging
from 100 to 350 meters, has over 200 glaciers in it and receives more than 7
meters of snowfall every year. Glaciers can be distinguished from regular snow
by the blue tinge they have. Glaciers melt and provide the head water for most
river systems. The Bow glacier is the origin of the Bow River. On the way there
were numerous stoppages for photographs and the most I liked were the ones at
the frozen lakes Hector and Bow. The ice was thin and walking on it was tricky.
A couple of tourists went knee deep and had some trouble pulling themselves
back. The reflection of Sun from the snow was so strong as to hurt the eyes.
Neil explained that the climatic conditions are so harsh that very few animals
and trees survived it. There were hardly 200 bears in the entire national park
of which 60 per cent were black bears and the rest grizzlies. The trees looked
small and stunted. It was astounding to be told that most of the trees were
between 300 and 400 years old. Poor soil conditions and the harsh weather kept
them that way. Another piece of interesting information was about the colour of
water in the lakes and river. The shimmer and hue were the result of rock flour
that were washed into the water bodies through glacial activity.
Neil
decided to distribute lunch at the Saskatchewan river crossing because it had a
lovely picnic place and adequate toilets. The river crossing was an important
trading post in the past for people going through to British Columbia. Neil
mentioned the yeoman services of David Thomson in mapping the rivers between
1785 and 1812. When the name was mentioned I reconnected with the Riverside
Park in Kamloops which lay on the confluence of the Thomson Rivers. The
pioneering work went largely unrecognised till more than a century later.
Through
all this interesting talk, scenic drive and photography sessions a lot of
information was gained and we reached the Athabasca Glacier and skywalk centre
without ever feeling that we had travelled over 180 km. At the Discovery Centre
Neil got us the ticket for the skywalk and arranged for transportation to the
Glacier. The group was transported to the place where the Ice Explorers were
parked in a 56 seater bus that belonged to the Brewster Company that ran the
facility at the glacier. The Ice Explorer is a humongous transport vehicle, the
like of which are only 24 in the whole world. Of this 22 are in Athabasca and
the balance are in Antarctica. Page, the comely girl who was behind the wheel
of the Ice Explorer, mentioned that each vehicle cost over C$ 2 million and
the 5 feet high tyres cost C$ 6000 apiece with each vehicle having 6 of them.
The drive down to the glacier in the glass topped vehicle is not for the faint-hearted. The sheer drop can only be taken by the traction of such a vehicle and
its top speed is 15 kph. On the way to the glacier I came across a new term –
Moraine. It is used to denote glacial debris. There are lateral and terminal moraines
depending on whether they are at the side or foot of the ice flow. The size of
moraines can vary from boulders to glacial flour.
The
Athabasca glacier is one of the six principal toes of the Columbia Icefields
and is the most visited glacier in North America. It is documented to having
receded by half in the past century and a quarter. The glacier cannot be
reached beyond a certain point because of hidden crevasses. It is said that
many tourists in the past have disappeared without a trace. Today the edge of
safe tourism is marked, beyond which tourists are prohibited to go. I was so
proud to see an Indian flag at the glacier and it was an hour to take a picture
holding the tri-colour.
The
Discovery Center vehicle dropped me off for the skywalk which is a km walk on
an informative board walk. The elliptical glass bottomed skywalk is over a 300
metre drop over the Sunwapta Valley. It took me quite some time to adapt to
watching the chasm beneath and walking ahead. It was indeed a most exhilarating
experience. Of course, the Grand Canyon skywalk was a more challenging
one. Once this was done it was time to
get back to the tour coach for the trip back to Banff. I slept most of the way
back having spent all my energies during the stupendous day. The most important
fact was that the weather was glorious all through the day. Not a drop of rain
fell nor did the clouds or mist play spoil sport. All in all, a most wonderful
excursion.
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